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contributor authorSheng Peng
contributor authorMark L. Brusseau
date accessioned2017-05-08T21:49:16Z
date available2017-05-08T21:49:16Z
date copyrightJuly 2012
date issued2012
identifier other%28asce%29he%2E1943-5584%2E0000535.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63402
description abstractThe relationship between air-water interfacial area and capillary pressure under higher water-content conditions is investigated for four natural porous media. The results show that the magnitude of the air-water interfacial area increases with increasing capillary pressure, consistent with the decrease in water saturation. The maximum observed air-water interfacial areas are dependent upon the magnitude of residual water saturation, which itself is condition-dependent. The more well-sorted porous-medium exhibited a greater rate of change of air-water interfacial area with capillary pressure than the more poorly sorted porous media. The observed relationship between air-water interfacial area and capillary pressure was quantified by coupling an empirical equation describing the air-water interfacial area versus water saturation relationship with the van Genuchten equation relating water saturation and capillary pressure. This equation produced reasonable simulations of the measured data.
publisherAmerican Society of Civil Engineers
titleAir-Water Interfacial Area and Capillary Pressure: Porous-Medium Texture Effects and an Empirical Function
typeJournal Paper
journal volume17
journal issue7
journal titleJournal of Hydrologic Engineering
identifier doi10.1061/(ASCE)HE.1943-5584.0000515
treeJournal of Hydrologic Engineering:;2012:;Volume ( 017 ):;issue: 007
contenttypeFulltext


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